Climate Change and Disasters

Regional changes of the severities of meteorological droughts and floods in India

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  • 1. Department of Engineering (GRO), University of Cambridge, Cambridge - CB2 1PZ, United Kingdom;
    2. Department of Engineering, University of Cambridge, Cambridge - CB2 1PZ, United Kingdom

Received date: 2009-09-28

  Revised date: 2010-07-10

  Online published: 2011-04-15

Abstract

The most important climatological feature of the South Asian region is the occurrence of monsoons. With increasing concerns about climate change, the need to understand the nature and variability of such climatic conditions and to evaluate possible future changes becomes increasingly important. This paper deals with long-term above and below normal monsoon precipitation causing prolong meteorological droughts and floods in India. Five regions across India comprising variable climates were selected for the study. Apart from long-term trends for individual regions, long-term trends were also calculated for the Indian region as a whole. The results show that intra-region variability for monsoon precipitation is large and there are increasing numbers of meteorological summer droughts. Meteorological monsoon floods were found to have negative long-term trends everywhere except in the peninsular Indian region. The results overall suggest generic conclusions concerning the region-wide long-term trend of severity of monsoon droughts and floods in India and their spatial variability.

Cite this article

Indrani Pal, Abir Al-Tabbaa . Regional changes of the severities of meteorological droughts and floods in India[J]. Journal of Geographical Sciences, 2011 , 21(2) : 195 -206 . DOI: 10.1007/s11442-011-0838-5

References

Bhalme H N, Mooley D A, 1980. Large scale droughts/floods and monsoon circulation. Monthly Weather Review,108: 1197-1211.
Bosilovich M G, Schubert S, Walker G, 2005. Global changes of the water cycle intensity. Journal of Climate, 18: 1591-1607.
Cislaghi M, De Michele C, Ghezzi A et al., 2005. Statistical assessment of trends and oscillations in rainfall dynamics:Analysis of long daily Italian series. Atmospheric Research, 77: 188-202.
Cruz R V, Harasawa H, Lal M et al., 2007. Asia. Climate change 2007: Impacts, adaptation and vulnerability. In:Parry M L, Canziani O F, Palutikof J P et al. (eds.), Contribution of Working Group II to the Fourth AssessmentReport of the Intergovernmental Panel on Climate Change. Cambridge, UK: Cambridge Univ. Press, 469-506.
Fisk D, 1997. Climate change and its impacts: A global perspective. In: Department of the Environment, Transport and the Regions, The Met Office Hadley Centre Brochure, UK.
Goswami B N, Venugopal V, Sengupta D et al., 2006. Increasing trend of extreme rain events over India in a warming environment. Science, 314: 1442-1445.
Kruger A C, 2006. Observed trends in daily precipitation indices in South Africa: 1910-2004. International Journal of Climatology, 26: 2275-2285.
Kumar A, Yang F, Goddard L et al., 2004. Differing trends in the tropical surface temperatures and precipitation over land and oceans. Journal of Climate, 17: 653-664.
Kumar P, Rupa Kumar K, Rajeevan M et al., 2007. On the recent strengthening of the relationship between ENSO and northeast monsoon rainfall over South Asia. Climate Dynamics, 28(6): 649-660.
Manton M J, Della-Marta P M, Haylock M R et al., 2001. Trends in extreme daily rainfall and temperature in Southeast Asia and the South Pacific: 1961-1998. International Journal of Climatology, 21: 269-284.
Murphy B F, Timbal B, 2008. A review of recent climate variability and climate change in south-eastern Australia.International Journal of Climatology, 28(7): 859-879.
New M, Todd M, Hulme M et al., 2001. Precipitation measurements and trends in the twentieth century. International Journal of Climatology, 21: 1899-1922.
Pal I, Al-Tabbaa A, 2008. Trends in seasonal precipitation extremes: An indicator of climate change. In: Final Proc. 7th European Conference on Applied Climatology (ECAC) 29 September-03 October 2008, Amsterdam,The Netherlands.
Pal I, Al-Tabbaa A, 2009. Trends in seasonal precipitation extremes: An indicator of ‘Climate Change’ in Kerala,India. Journal of Hydrology, 367: 62-69.
Pal I, Al-Tabbaa A, 2010a. Monsoon rainfall extreme indices and tendencies from 1954-2003 in Kerala, India.Climatic Change. (in press)
Pal I, Al-Tabbaa A, 2010b. Regional changes in extreme monsoon rainfall deficit and excess in India. Dynamics of Atmospheres and Oceans, 49: 206-214.
Pal I, Al-Tabbaa A, 2010c. Long-term changes and variability of monthly extreme temperatures in India. Theoretical and Applied Climatology, 100(1): 45-56.
Palmer T N, Raisanen J, 2002. Quantifying the risk of extreme seasonal precipitation events in a changing climate. Nature, 415: 512-514.
Pant G B, Rupa Kumar K, 1997. Climates of South Asia. John Wiley and Sons, England.
Sen Roy S, Balling J R, 2004. Trends in extreme daily precipitation indices in India. International Journal of Climatology, 24: 457-466.
Soman M K, Krishna Kumar K, Singh N, 1988. Decreasing trend in the rainfall of Kerala. Current Science, 57(1): 7-12.

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